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Selected Exhibitions : 2008 /"The Third Guangzhou Triennial : Farewell to Post-Colonialism", Guangdong Museum of Art, Guangzhou,China / 2007 /"Alchemy of Shadow : 3rd Lianzhou International Photo Festival", Lianzhou, China / 2006 /"A Yellow Box In Qingpu: Contemporary Art and Architecture in a Chinese Space", Shanghai /"Micrology, the Politics of Realism Chinese Contemporary Art Exhibition, Macao / 2005 /"In the Depth of Reality : China Contemporary Art Exhibition", Hangzhou /"Gift, Contemporary Art Invited Exhibition", Hangzhou / 2004 /"Formatting: New Media Art Project", Hangzhou /"Labyrinth : the Second Chinese New Media Art Festival", Hangzhou / 2003 /"Experimental Art Project in White Pagoda Mountain", Hangzhou /"Links: Contemporary Art Exhibition", Hangzhou /"Exhibition of Chinese Young Artists, Hangzhou

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The study of the geological characteristics, ore-forming condition and genetic type from the Pingdingshan gold deposit, shows that the cryptomerous diorite and dioritic porphyrite in different stages formed a vein rock zone with gold containing ore bodies in the area, and five vein ore bodies were blocked out by spreading out with the NNE direction in the field.

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Lithologic character of Eogene syste is interbedded sandstone and mudstone primarily, including the thin layer oil shale, Neocene- Quaternary system is set of rivers deposits. Based on this, through the reaserch of ateral correlation and distribution characteristics of every structural layers show that: Paleozoic synthem overall thickness of relatively stable.The residual thickness of Mesozoic synthem is difference in the horizontal, Residues in the horizontal thickness of greater difference, to the greatest thickness achieve to 4500m. Eogene syste has obviously fault depression basin deposition characteristic, the thickness of many sags achieve to 3000 m ,from Neocene, the stratum crosswise mop tended to be stable.

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On the basis of sand-bodies Isopach figure drawing, the distribution of major reservoir sand-bodies of Neopaleozoic in south of North China Basin was studied. Basing on the distribution of sand-bodies in sequence stratigraphic framework, combining the development and distribution features of barrier and underwater distributary channel, there is a disquisition on the distribution regularity of pay reservoir sand-bodies of Neopaleozoic in this area.

以編制砂體等厚圖的方式研究了華北盆地南部上古生界主要儲集砂體的平面展布規(guī)律无码有码日韩制服AV，并以層序地層格架下的砂體展布研究為基礎(chǔ)亚洲日韩色图10p，從沉積體系控制下的砂體分布特點出發(fā)，結(jié)合障壁島與水下分流河道的發(fā)育與分布特點日韩人人操人人射，系統(tǒng)深入地開展了區(qū)內(nèi)上古生界有利儲集砂體的分布規(guī)律研究性XX18。

Based on the date of outcrop, log and lithology, sequence stratigraphic division and correlation were made on Neopaleozoic in south of North China Basin, and high-precision geologic correlation framework was built up in the basin.2. In the term of sedimentary features of Neopaleozoic in south of North China Basin, lateral variation of sedimentary facies was studied selectively in Benxi-Taiyuan Formation, Shanxi Formation, Lower Shihezi Formation, Upper Shihezi Formation and Shiqianfeng Formation. Lithofacies paleographic features and the sedimentary evolutionary process of Late Paleozoic in south of North China Basin were worked also.3. On the basis of sand-bodies Isopach figure drawing, the distribution of major reservoir sand-bodies of Neopaleozoic in south of North China Basin was studied. Basing on the distribution of sand-bodies in sequence stratigraphic framework, combining the development and distribution features of barrier and underwater distributary channel, there is a disquisition on the distribution regularity of pay reservoir sand-bodies of Neopaleozoic in this area.

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